Results 181 to 190 of about 4,473 (252)
Geochemical Characteristics of Mafic granulites and Associated Websterites from the Sittampundi Complexsouth India [PDF]
B.V.C. Moses +2 more
core
Some of the next articles are maybe not open access.
Related searches:
Related searches:
A new model for chromitite formation in ophiolites: Fluid immiscibility
Science China Earth Sciences, 2020Chen Chen, Yan Xiao, Ibrahim Uysal
exaly +2 more sources
Canadian Mineralogist, 2022
The abundance of Ru in chromite has been suggested as an indicator of sulfide liquid saturation in komatiites. The komatiite magma-derived Archean Coobina intrusion is known to be barren in terms of sulfide mineralization.
L. Schoneveld +4 more
semanticscholar +1 more source
The abundance of Ru in chromite has been suggested as an indicator of sulfide liquid saturation in komatiites. The komatiite magma-derived Archean Coobina intrusion is known to be barren in terms of sulfide mineralization.
L. Schoneveld +4 more
semanticscholar +1 more source
Lithos, 2021
Abstract Podiform chromitites are unique rock units of ophiolites and ophiolitic melanges and represent invaluable repositories that reliably record the formation environment and evolution of their source and host rocks. However, there are relatively few podiform chromitites reported from Archean terranes. Here we document the major, minor, and trace
Yang Huang +8 more
semanticscholar +2 more sources
Abstract Podiform chromitites are unique rock units of ophiolites and ophiolitic melanges and represent invaluable repositories that reliably record the formation environment and evolution of their source and host rocks. However, there are relatively few podiform chromitites reported from Archean terranes. Here we document the major, minor, and trace
Yang Huang +8 more
semanticscholar +2 more sources
Amphibole as a witness of chromitite formation and fluid metasomatism in ophiolites
American Mineralogist, 2022Here we present new occurrences of amphibole in a suite of chromitites, dunites, and harzburgites from the mantle sequence of the Lycian ophiolite in the Tauride Belt, southwest Turkey.
Qihui Pan +7 more
semanticscholar +1 more source
Canadian Mineralogist, 2021
The UG-2 chromitite layer, with its elevated platinum-group element content, is a key marker horizon in the eastern and western limbs of the Bushveld Igneous Complex and the largest platinum-group element chromite-hosted resource of its kind in the ...
Malose M. Langa +3 more
semanticscholar +1 more source
The UG-2 chromitite layer, with its elevated platinum-group element content, is a key marker horizon in the eastern and western limbs of the Bushveld Igneous Complex and the largest platinum-group element chromite-hosted resource of its kind in the ...
Malose M. Langa +3 more
semanticscholar +1 more source
Peridotites, chromitites and diamonds in ophiolites
Nature Reviews Earth & Environment, 2021Ophiolites, which represent segments of oceanic lithosphere obducted onto the continental crust, provide an important window into processes such as continental rifting, mantle melting, asthenospheric upwelling and cooling of oceanic lithosphere. Traditionally, research has focused on crustal sections of ophiolites.
Jingsui Yang +3 more
openaire +1 more source
Canadian Mineralogist, 2021
Nearly monomineralic stratiform chromitite seams of variable thickness (millimeters to meters) occur in many of the world's layered mafic-ultramafic intrusions. These seams are often associated with economically significant quantities of platinum group
Emma J. Hunt, B. O’Driscoll, J. Day
semanticscholar +1 more source
Nearly monomineralic stratiform chromitite seams of variable thickness (millimeters to meters) occur in many of the world's layered mafic-ultramafic intrusions. These seams are often associated with economically significant quantities of platinum group
Emma J. Hunt, B. O’Driscoll, J. Day
semanticscholar +1 more source